DOCSLIB.ORG

Sedimentary Framework of the Western Gulf of Maine and the Southeastern Massachusetts Offshore Area

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Sedimentary Framework of the Western Gulf of Maine and the Southeastern Massachusetts Offshore Area 7 Sedimentary Framework of the Western Gulf of Maine and the Southeastern Massachusetts Offshore Area ~ ....,------------------------------------ ZU· G E 0 L 0 G I c A L s u R v E y p R 0 F E s s I 0 N A L p A p E R 7 5 7 oo) -13 75-7 Sedimentary Framework of the Western Gulf of Maine and the Southeastern Massachusetts Offshore Area By R. N. OLDALE, ELAZAR UCHUPI, and K. E. PRADA ~---------------------------------------------------- [0$ G E 0 L 0 G I C A L S U R V E Y P R 0 F E S S I 0 N A L P A P E R 7 5 7 Four sedimentary units ranging in age from Cretaceous to Holocene have been inferred from a seismic survey J and a preglacial drainage system has been delineated UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600378 For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 Price: Paper Cover- $1.75, domestic postpaid; $1.50, GPO Bookstore. Stock No. 2401~0304 CONTENTS Pase J\bstract ---------------------------------------------------------------- 1 Introduction ------------------------------------------------------------- 1 J\cknowledgT.nents ---------------------------------------------------- 3 Methods of investigation -------------------------------------------------- 3 Interpretation of seismic profiles ------------------------------------------- 8 Bathymetry --------------------------------------------------------- 3 Basement ----------------------------------------------------------- 4 Inferred coastal-plain deposits ----------------------------------------- 4 Inferred moraine deposits -------------------------------------------- 5 Glaciomarine and marine deposits ------------------------------------- 5 Glaciolacustrine deposits ---------------------------------------------- 6 Total sediment thickness and basement structure ----------------------- 6 Geologic history --------------------------------------------------------- 7 References -------------------------------------------------------------- 8 Economic deposits -------------------------------------------------------- 9 ILLUSTRATIONS Pqe PLATE 1. Generalized surficial geologic map and interpretive geologic sections of seismic profiles, western Gulf of Maine and southeastern Massachusetts offshore area ------------------------------------------In pocket 2. Reconnaissance isopach maps of bottom sediments and structure contour map of basement surface of the western Gulf of Maine and southeastern Massachusetts offshore area --------------------------- In pocket FIGURE 1. Map showing bathymetry of the continental margin off northeastern United States and Nova Scotia ____ 2 n1 SEDIMENTARY FRAMEWORK OF THE WESTERN GULF OF MAINE AND THE SOUTHEASTERN MASSACHUSETTS OFFSHORE AREA 1 By R. N. 0LDALE, ELAZAR U CHUPI,2 and K. E. P~A2 ABSTRACT (fig. 1) and consists of the Gulf of Maine, a broad 2 The sedimentary framework of the western Gulf of Maine 90, 700-km lowland, and Georges Bank, which sep­ and the southeastern Massachusetts offshore area has been arates the gulf from the open ocean. Northeast and interpreted from data obtained with a seismic profiler, supple­ Great South Channels provide passageways from the mented by information from geology on land and from sam­ Gulf of Maine to the Atlantic Ocean. Cape Cod Bay, ples offshore. A geologic map, three generalized isopach maps, Nantucket Sound, and Buzzards Bay make up and a generalized contour map of the basement surface provide significant information relative to the framework. smaller lowlands. Four sedimentary units have been distinguished on the basis The floor of the Gulf of Maine is extremely irreg­ of seismic data and are inferred to be: (1) coastal-plain ular -and is marked by deep basins, low swells, sediments of Late Cretaceous to early Pleistocene age, (2) ridges, and flat-topped banks and ledges (Uchupi, moraine deposits of Pleistocene age, (3) glaciomarine and 1968). In an early study, Johnson (1925, p. 264- marine deposits of Pleistocene and Holocene age, and (4) glaciolacustrine deposits ·of late Pleistocene age. The distribu­ 296) suggested that the Gulf of Maine was carved tion of the inferred coastal-plain deposits delineates drainage out of continental-shelf strata by stream erosion. He systems whose streams are believed to have carved the fol­ further stated that the basins within the gulf mark lowing features out of the coastal-plain and the shelf strata: positions of former stream valleys and that North­ the Gulf of Maine, the- cuesta beneath Georges Bank, and east and Great South Channels were the water gaps the islands off southern New England. This erosion is be­ lieved to have taken place during late Tertiary or early of the two major streams of the drainage systems. Pleistocene time. The inferred moraine deposits overlie base­ The topographic highs within the gulf were inter­ ment rocks or the unconformity on the coastal-plain deposits; preted by him as subordinate cuestas within the low­ they define stages in the retreat of the last glacier in coastal land. He also believed that Georges Bank was a New England. The acoustic unit assigned to the glaciomarine cuesta cut in coastal-plain strata. and marine deposits. is believed to represent in part glacial rock flour carried into the marine environment by melt-water The wide occurrence of glacial deposits in the streams and in part silt and clay winnowed from the banks Gulf of Maine and the observation that the type of and ledges during the postglacial rise in sea level. The in­ topography found off New England appears to be ferred glaciolacustrine deposits are thought to have been restricted ~ formerly glaciated coasts led Shepard, deposited in Cape Cod Bay during the retreat of the last ice Trefethen, and Cohee (1934) to suggest that glacial in that area. erosion played a significant role in the formation of the gulf. On the basis of data obtained with a con­ INTRODUCTION tinuous seismic profiler, Uchupi (1966) and Oldale Continental shelves of northern latitudes are topo­ and Uchupi (1970) suggested that the Gulf of Maine graphically very irregular and are characterized by probably was formed by a combination of preglacial lowlands along the coast, U-shaped troughs extend­ fluvial erosion and Pleistocene glacial erosion. Using ing from shore to the shelf's edge, and a chain of data from these profiles, Oldale and Uchupi (1970) banks along the outer edge of the shelf ( Holtedahl, were able to trace the preglacial fluvial systems that 1958). This type of shelf occurs off New England eroded the Gulf of Maine. Interpretation of seismic profiles also suggests that some of the basins are 1 Contribution 2669 of the Woods Hole Oceanographic Institution, based on work done under a program eondueted jointly by the U.S. Geological underlain by steeply dipping strata which acoustic­ Survey and the Woods Hole Oceanographic Institution and financed by ally resemble known Triassic sedimentary rocks in the U.S. Geological Survey. • Woods Hole Oceanographic Institution, Woods Bole, :Mass. the Gulf of Maine and the Bay of Fundy ( Tagg and 1 2 SEDIMENTARY FRAMEWORK OFFSHORE AREA, MAINE AND MASSACHUSETTS 72" + + + + s + GE. + 0~ G~ 0 25 50 75 100 NAUTICAL MILES I I I I I I I I I 0 25 50 75 100 KILOMETERS Ill II I I I I CONTOURS IN METERS FIGURE !.-Bathymetry of the continental margin off northeastern United States and Nova Scotia. Bathymetry from Uchupi ,1965). Uchupi, 1966; Uchupi, 1966). This interpretation continental shelf. The first area chosen for more led Oldale and Uchupi ( 1970) to speculate that the detailed study was the westernmost part of the Gulf larger basins within the gulf represent Triassic of Maine (fig. 1). The large amount of seismic fault basins modified to their present shape by profiler data collected witl:tin this relatively small fluvial and glacial erosion. area has made possible the refinement of the recon­ Most of these earlier studies were based on widely struction of the sedimentary framework of the cen­ spaced seismic profiler records ; consequently, the tral New England offshore area. Because the geo­ sedimentary framework of the offshore area could logic formations that are segregated on the basis of be reconstructed only in the broadest sense. With their acoustical-reflection properties are mostly in­ completion of a reconnaissance survey of the At­ accessible to direct observation, the geologic inter­ lantic continental margin of the United States, the pretation of seismic profiles relies heavily on in­ U.S. Geological Survey, in cooperation with the ference. Most of the unit identifications in this Woods Hole Oceanographic Institution, began a report, therefore, are referred to as "inferred." more detailed geologic mapping program of the Seismic surveys are, however, the most expedient INTRODUCTION 3 means of reconnoitering a marine area for struc­ output impedance was suitable for driving as much tural and stratigraphic information. They provide a as 600 m of tow cable, while the 20 db provided basis for planning and carrying out more specific signals greater in amplitude than any tow noise geologic investigations whose results may prove or generated by the tow cable. A broad-band monolithic disprove the inferences that were made from the amplifier with gain variable to 40 db amplified the seismic data. received signal. This signal was then fed to suitable line drivers, filtered passively, and recorded on a ACKNOWLEDGMENTS
Load more

Recommended publications
  • Enormous Carnivores, Microscopic Food, and a Restaurant That's Hard to Find
    Enormous Carnivores, Microscopic Food, and a Restaurant That's Hard to Find MARK F. BAUMGARTNER, CHARLES A. MAYO, AND ROBERT D. KENNEY April 1986 Cape Cod Bay We'd known for a long time that there were places east of Cape Cod where pow+l tidal impulses meet the sluggiih southward-moving coastal cur- rent, places where right whales lined up along the rips where plankton con- centrate. On a windless day in early April 1986, we decided to see ifright whales hadfoundsuch an area. The winter season, when right whales come to Cape Cod, had been a hard one, and calm hys like this were few, so we could at last get to the more distant convergence and, as localjshermen do, see what we could catch. It was gloomy and nearly dzrk when we lefi the port. For those of us who study whales, expectations are usually tempered by realip; we were lookingfor one of the rarest of all mammals in the shroud of the ocean. To- day, however, spirits were high as the hybreak was filed with springtime promise. Along the great outer beach of the Cape, so close to shore that we couldsmell the land nearb, thefist right whale was spotted working along one of those current rips. And as the sun climbed out of the haze, the whale rose and opened that great and odd mouth and skimmed the su$ace in a silence broken only ly the sizzle of water passing through its huge filtering Enormous Carnivores, Microscopic Food 139 apparatus. Our earlier optimism was warranted, andfor several hours we drzFedjust clear of the linear rip that the whale was working, recording the complex pattern of its movements.
    [Show full text]
  • Evaluation of Northern Right Whale Ship Strike Reduction Measures in the Great South Channel of Massachusetts
    NOAA Technical Memorandum NMFS-NE-202 Evaluation of Northern Right Whale Ship Strike Reduction Measures in the Great South Channel of Massachusetts U. S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Marine Fisheries Service Northeast Fisheries Science Center Woods Hole, Massachusetts March 2007 Recent Issues in This Series: 184. A Large Marine Ecosystem Approach to Fisheries Management and Sustainability. By Frank J. Gable. August 2004. v + 84 p., 38 figs., 10 tables. NTIS Access. No. PB2005-101435. [Online publication only.] 185. Revised and Updated Edition of F. Bruce Sanford's 1957 "Planning Your Scientific Research Paper." By Jon A. Gibson. August 2004. x + 36 p., 5 figs., 12 tables. NTIS Access. No. PB____-______. 186. Essential Fish Habitat Source Document: Silver Hake, Merluccius bilinearis, Life History and Habitat Characteristics. 2nd ed. By Meredith C. Lock and David B. Packer. August 2004. v + 68 p., 28 figs., 6 tables. NTIS Access. No. PB2005-101436. [Online publication only.] 187. Essential Fish Habitat Source Document: American Plaice, Hippoglossoides platessoides, Life History and Habitat Character- istics. 2nd ed. By Donna L. Johnson. August 2004. vi + 72 p., 23 figs., 6 tables. NTIS Access. No. PB2006-102421. [Online publication only.] 188. Northeast Regional Commercial Fishing Input-Output Model, by Scott R. Steinback and Eric M. Thunberg. NTIS Access. No. PB2007-104394. April 2006. v + 54 p., 2 figs, 15 tables. [Online publication only.] 189. Essential Fish Habitat Source Document: Sea Scallop, Placopecten magellanicus, Life History and Habitat Characteristics. 2nd ed. By Deborah R. Hart and Antonie S. Chute. September 2004. v + 21 p., 6 figs., 2 tables.
    [Show full text]
  • Line 5 Straits of Mackinac Summary When Michigan Was Granted
    Line 5 Straits of Mackinac Summary When Michigan was granted statehood on January 26, 1837, Michigan also acquired ownership of the Great Lakes' bottomlands under the equal footing doctrine.1 However before Michigan could become a state, the United States first had to acquire title from us (Ottawa and Chippewa bands) because Anglo-American law acknowledged that we owned legal title as the aboriginal occupants of the territory we occupied. But when we agreed to cede legal title to the United States in the March 28, 1836 Treaty of Washington ("1836 Treaty", 7 Stat. 491), we reserved fishing, hunting and gathering rights. Therefore, Michigan's ownership of both the lands and Great Lakes waters within the cession area of the 1836 Treaty was burdened with preexisting trust obligations with respect to our treaty-reserved resources. First, the public trust doctrine imposes a duty (trust responsibility) upon Michigan to protect the public trust in the resources dependent upon the quality of the Great Lakes water.2 In addition, Art. IV, § 52 of Michigan's Constitution says "conservation…of the natural resources of the state are hereby declared to be of paramount public concern…" and then mandates the legislature to "provide for the protection of the air, water and other natural resources from 3 pollution, impairment and destruction." 1 The State of Michigan acquired title to these bottomlands in its sovereign capacity upon admission to the Union and holds them in trust for the benefit of the people of Michigan. Illinois Central Railroad Co. v. Illinois, 146 U.S. 387, 434-35 (1892); Nedtweg v.
    [Show full text]
  • Lighthouses – Clippings
    GREAT LAKES MARINE COLLECTION MILWAUKEE PUBLIC LIBRARY/WISCONSIN MARINE HISTORICAL SOCIETY MARINE SUBJECT FILES LIGHTHOUSE CLIPPINGS Current as of November 7, 2018 LIGHTHOUSE NAME – STATE - LAKE – FILE LOCATION Algoma Pierhead Light – Wisconsin – Lake Michigan - Algoma Alpena Light – Michigan – Lake Huron - Alpena Apostle Islands Lights – Wisconsin – Lake Superior - Apostle Islands Ashland Harbor Breakwater Light – Wisconsin – Lake Superior - Ashland Ashtabula Harbor Light – Ohio – Lake Erie - Ashtabula Badgeley Island – Ontario – Georgian Bay, Lake Huron – Badgeley Island Bailey’s Harbor Light – Wisconsin – Lake Michigan – Bailey’s Harbor, Door County Bailey’s Harbor Range Lights – Wisconsin – Lake Michigan – Bailey’s Harbor, Door County Bala Light – Ontario – Lake Muskoka – Muskoka Lakes Bar Point Shoal Light – Michigan – Lake Erie – Detroit River Baraga (Escanaba) (Sand Point) Light – Michigan – Lake Michigan – Sand Point Barber’s Point Light (Old) – New York – Lake Champlain – Barber’s Point Barcelona Light – New York – Lake Erie – Barcelona Lighthouse Battle Island Lightstation – Ontario – Lake Superior – Battle Island Light Beaver Head Light – Michigan – Lake Michigan – Beaver Island Beaver Island Harbor Light – Michigan – Lake Michigan – St. James (Beaver Island Harbor) Belle Isle Lighthouse – Michigan – Lake St. Clair – Belle Isle Bellevue Park Old Range Light – Michigan/Ontario – St. Mary’s River – Bellevue Park Bete Grise Light – Michigan – Lake Superior – Mendota (Bete Grise) Bete Grise Bay Light – Michigan – Lake Superior
    [Show full text]
  • High-Resolution Seismic-Reflection Surveys in the Nearshore of Lower
    U.S. DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY HIGH-RESOLUTION SEISMIC-REFLECTION SURVEYS IN THE NEARSHORE OF OUTER CAPE COD, MASSACHUSETTS David S. Foster and Lawrence J. Poppe U.S. Geological Survey Woods Hole, MA 02543 Open-File Report 03-235 May 2003 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. Table of Contents Introduction Previous Work Geologic Setting Data Acquisition and Processing Seismic-Reflection Interpretation Integration with Land-based Stratigraphy Conclusions Acknowledgements References Cited Introduction The U.S. Geological Survey (USGS) Woods Hole Field Center (WHFC), in cooperation with the USGS Water Resources Division conducted high-resolution seismic-reflection surveys along the nearshore areas of outer Cape Cod, Massachusetts from Chatham to Provincetown, Massachusetts (Fig. 1). The objectives of this investigation were to determine the stratigraphy of the nearshore in relation to the Quaternary stratigraphy of outer Cape Cod by correlating units between the nearshore and onshore and to define the geologic framework of the region. Previous Work Earlier seismic-reflection surveys of Cape Cod Bay and east of Cape Cod began with Hoskins and Knott (1961) who collected high-resolution seismic profiles in Cape Cod Bay and defined a seismic stratigraphic framework of the region. Oldale and O’Hara (1990) established the relationship of the onshore regional geology of the Cape (Oldale, 1982) and the stratigraphy of the Gulf of Maine to the seismic stratigraphy of Cape Cod Bay.
    [Show full text]
  • CPB1 C10 WEB.Pdf
    338 ¢ U.S. Coast Pilot 1, Chapter 10 Chapter 1, Pilot Coast U.S. 70°45'W 70°30'W 70°15'W 71°W Chart Coverage in Coast Pilot 1—Chapter 10 NOAA’s Online Interactive Chart Catalog has complete chart coverage http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 71°W 13279 Cape Ann 42°40'N 13281 MASSACHUSETTS Gloucester 13267 R O B R A 13275 H Beverly R Manchester E T S E C SALEM SOUND U O Salem L G 42°30'N 13276 Lynn NORTH ATLANTIC OCEAN Boston MASSACHUSETTS BAY 42°20'N 13272 BOSTON HARBOR 26 SEP2021 13270 26 SEP 2021 U.S. Coast Pilot 1, Chapter 10 ¢ 339 Cape Ann to Boston Harbor, Massachusetts (1) This chapter describes the Massachusetts coast along and 234 miles from New York. The entrance is marked on the northwestern shore of Massachusetts Bay from Cape its eastern side by Eastern Point Light. There is an outer Ann southwestward to but not including Boston Harbor. and inner harbor, the former having depths generally of The harbors of Gloucester, Manchester, Beverly, Salem, 18 to 52 feet and the latter, depths of 15 to 24 feet. Marblehead, Swampscott and Lynn are discussed as are (11) Gloucester Inner Harbor limits begin at a line most of the islands and dangers off the entrances to these between Black Rock Danger Daybeacon and Fort Point. harbors. (12) Gloucester is a city of great historical interest, the (2) first permanent settlement having been established in COLREGS Demarcation Lines 1623. The city limits cover the greater part of Cape Ann (3) The lines established for this part of the coast are and part of the mainland as far west as Magnolia Harbor.
    [Show full text]
  • Shallow Structure
    IBRARY CO Atlantic Continental Shelf and Slope of the United States Shallow Structure GEOLOGICAL SURVEY PROFESSIONAL PAPER 529·1 Atlantic Continental . r.. Shelf and Slope of The United States- Shallow Structure By ELAZAR UCHUPI GEOLOGICAL SURVEY PROFESSIONAL PAPER 529-I Description of the subsurface morphology of the shelf and slop~ (continental terrace) ·and some speculations on the evolution of the sedimentary framework of the terrace UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1970 • UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1 (paper cover) CONTENTS P11ge Pllge Abstract------------------------------------------- 11 Continental shelf from Cape lioa to Virginia___________ 113 Introduction---------------------~----------------- 1 Continental slope from· Georges Bank to Cape Hatteras_ 15 Acknowledgments _____________________________ _ 2 Continental shelf from Cape Hatteras to Cape Romain___ 19 Topographic setting ___________________ --- _____ ---- __ 2 Blake Plateau area__________________________________ 19 Methods of study __________________________________ _ 2 Straits of Florida ___________ :... _______________ :._______ 30 Scotian Shelf area _________________________________ _ 5 Geologic maP-------------------------------------- 31 5 Isopach maps_ _ _ _ _ __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 33 Gulf of Maine and Bay of
    [Show full text]
  • Boston Harbor Drained: a Case Study Using Hydrographic Systems to Assess Potential Cultural Resource Sites
    Transactions on the Built Environment vol 65, © 2003 WIT Press, www.witpress.com, ISSN 1743-3509 Boston Harbor drained: a case study using hydrographic systems to assess potential cultural resource sites J. Weirich Ofice of Ocean Exploration, National Oceanic and Atmospheric Administration, USA Abstract A recent navigation project in Boston Harbor, Massachusetts illustrated the use of different hydrographic techniques in assessing cultural resources. The NOAA Ship WHITING, a hydrographic research vessel for the U.S. Department of Commerce's, National Oceanic and Atmospheric Administration, surveyed the entire harbor and its approaches. The main goal of the project was to update the nautical charts for safe navigation. However, the hydrographic team also addressed areas of cultural significance, with particular attention paid to the inner harbor waterfront, the harbor's islands, and shipwrecks located in the waterways. Several remote sensing techniques were used; tools and expertise that are currently being under utilized by the submerged cultural resource community. This paper does not highlight the history of Boston Harbor, but rather use it as a backdrop for how best to survey an historical harbor given the appropriate tools and proper planning. It also stresses the need for archaeological expertise in hydrographic surveying. 1 Introduction National Oceanic and Atmospheric Administration (NOAA), under the U.S. Department of Commerce, is responsible for charting the US coastlines and ports. Analogous agencies to NOAA include the Canadian Hydrographic Service and the United Kingdom Hydrographic Office. NOAA acquires bathymetric data, processes it and creates nautical charts used by mariners throughout the world. NOAA targets major ports to frequently survey to assess Transactions on the Built Environment vol 65, © 2003 WIT Press, www.witpress.com, ISSN 1743-3509 40 Maritime Heritage any charges in the bathymetry, or bottom features, so that charts can be updated for safe navigation.
    [Show full text]
  • 2008 Salem Harbor Plan Substitution Summary 122 Table 3: 2008 Salem Harbor Plan Amplification Summary 123
    SALEM HARBOR PLAN The City of Salem, Massachusetts Mayor Kimberley Driscoll January 2008 Fort Point Associates, Inc TABLE OF CONTENTS LIST OF FIGURES AND TABLES ii ACKNOWLEDGEMENTS iii 2008 UPDATE OVERVIEW iv I. SUMMARY Introduction 1 The Vision 1 II. INTRODUCTION Overview 4 The Harbor Planning Area 4 The Planning Process 6 A Guide to the Planning Recommendations 9 III. FRAMEWORK FOR PLANNING Summary of Existing Conditions 13 Goals and Objectives 20 IV. PLANNING RECOMMENDATIONS Area-Wide Recommendations 24 South Commercial Waterfront 38 Tourist Historic Harbor 49 North Commercial Waterfront 56 Industrial Port 60 Community Waterfront 63 V. IMPLEMENTATION Oversight and Responsibilities 71 Economic Development 76 Phasing Strategy 78 Resources 80 Implementation - Summary of Proposed Actions 88 VI. REGULATORY ENVIRONMENT Overview: Chapter 91 100 Activities Subject to Chapter 91 102 Designated Port Area 103 Authority of the Salem Harbor Plan and DPA Master Plan 104 Guidance to DEP: Substitute Provisions 105 Guidance To DEP: Non-substitute Provisions 111 Other Local and Federal Regulations and Permits 117 Substitution and Amplification Tables 122 VII. FUTURE PLANNING 124 i APPENDICES A. PUBLIC INPUT - STAKEHOLDER INTERVIEWS B. RECENTLY OR SOON TO BE COMPETED REPORTS Salem Open Space and Recreation Plan (2007) Winter Island Barracks Building Feasibility Reuse Study (Jul 2007) Downtown Salem Retail Market Study: Strategy and Action Plan (May 2007) Salem Wharf Expansion Plan (expected early 2008) C. ENVIRONMENTAL RESOURCE ENHANCEMENT D. BATHYMETRIC
    [Show full text]
  • Annual Report of the Board of Harbor
    Nil ill U I I III iii!!ili!!iill!IIHIIililllll!!il!IJilti! I !in liiiliy I; ' ini!H!;ihiitiii;iituii!iiiiii!'iii(rii i!ii: . s-i i ji n ijl! ii!IHi!iiii!llliilliilJiiillillllll!ill!!tlliiiii!iii!ii)iliiiiiiitilitiit i r n COLLECTiON m 1 2 isso 'niyersity of Massachusetts Deposifory Copy : PUBLIC DOCUMENT .... .... No. U. ANNUAL EEPOKT Board of Harbor and Land Commissioners For the Year 189 7. BOSTON WRIGHT & POTTER PRINTING CO., STATE PRINTERS, 18 Post Office Square. 1898. Digitized by the Internet Archive in 2011 with funding from Boston Library Consortium IVIember Libraries http://www.archive.org/details/annualreportofbo1897boar Commonlwalt^ ai P^assat^usftts. REPORT. To the Honorable the Seriate and House of Representatives of the Common- wealth of Massachusetts. The Board of Harbor and Land Commissioners, pursuant to the provisions of law, respectfully submits its annual re- port for the year 1897, covering a period of twelve months, from Nov. 30, 1896. Every year brings an access of business of a character which needs the personal attention of the commissioners. Every new subject matter over which the Board is given jurisdiction, or with reference to which an examination and report is required, brings with it a multitude of lesser re- quirements, such as the visitation of localities, conferences with individuals, examination of documents and answers to inquiries from others, which take up time. In systematizing the business of the office, the Board has found it convenient to have a return day, on which parties petitioning may come in and be heard, either in person, or, as often happens, by counsel, whereby the hearings are now and again extended by continuances, in which questions of law and fact are presented and argued, and have to be finally determined by the Board.
    [Show full text]
  • 536 Part 117—Drawbridge Operation Regulations
    Pt. 117 33 CFR Ch. I (7–1–12 Edition) (c) Any Order of Apportionment 117.47 Clearance gages. made or issued under section 6 of the 117.49 Process of violations. Truman-Hobbs Act, 33 U.S.C. 516, may be reviewed by the Court of Appeals for Subpart B—Specific Requirements any judicial circuit in which the bridge 117.51 General in question is wholly or partly located, 117.55 Posting of requirements. if a petition for review is filed within 90 117.59 Special requirements due to hazards. days after the date of issuance of the ALABAMA order. The review is described in sec- tion 10 of the Truman-Hobbs Act, 33 117.101 Alabama River. U.S.C. 520. The review proceedings do 117.103 Bayou La Batre. 117.105 Bayou Sara. not operate as a stay of any order 117.107 Chattahoochee River. issued under the Truman-Hobbs Act, 117.109 Coosa River. other than an order of apportionment, 117.113 Tensaw River. nor relieve any bridge owner of any li- 117.115 Three Mile Creek. ability or penalty under other provi- sions of that act. ARKANSAS 117.121 Arkansas River. [CGD 91–063, 60 FR 20902, Apr. 28, 1995, as 117.123 Arkansas Waterway-Automated amended by CGD 96–026, 61 FR 33663, June 28, Railroad Bridges. 1996; CGD 97–023, 62 FR 33363, June 19, 1997; 117.125 Black River. USCG–2008–0179, 73 FR 35013, June 19, 2008; 117.127 Current River. USCG–2010–0351, 75 FR 36283, June 25, 2010] 117.129 Little Red River.
    [Show full text]
  • Department of Commerce
    Vol. 80 Friday, No. 34 February 20, 2015 Part II Department of Commerce National Oceanic and Atmospheric Administration 50 CFR Part 226 Endangered and Threatened Species; Critical Habitat for Endangered North Atlantic Right Whale; Proposed Rule VerDate Sep<11>2014 17:36 Feb 19, 2015 Jkt 235001 PO 00000 Frm 00001 Fmt 4717 Sfmt 4717 E:\FR\FM\20FEP2.SGM 20FEP2 TKELLEY on DSK3SPTVN1PROD with PROPOSALS2 9314 Federal Register / Vol. 80, No. 34 / Friday, February 20, 2015 / Proposed Rules DEPARTMENT OF COMMERCE Regional Office, 55 Great Republic This critical habitat was revised in 2006 Drive, Gloucester, MA 01930. to include two foraging areas in the National Oceanic and Atmospheric Instructions: You must submit North Pacific Ocean—one in the Bering Administration comments by one of the above methods Sea and one in the Gulf of Alaska (71 to ensure that we receive, document, FR 38277; July 6, 2006). 50 CFR Part 226 and consider them. Comments sent by In 2006, we published a comprehensive right whale status [Docket No. 100217099–4774–02] any other method, to any other address or individual, or received after the end review, which concluded that recent RIN 0648–AY54 of the comment period, may not be genetic data provided unequivocal considered. All comments received are support to distinguish three right whale Endangered and Threatened Species; a part of the public record and will lineages as separate phylogenetic Critical Habitat for Endangered North generally be posted to http:// species (Rosenbaum et al. 2000): (1) The Atlantic Right Whale www.regulations.gov without change. North Atlantic right whale (Eubalaena AGENCY: National Marine Fisheries All Personal Identifying Information (for glacialis) ranging in the North Atlantic Service (NMFS), National Oceanic and example, name, address, etc.) Ocean; (2) The North Pacific right whale Atmospheric Administration (NOAA), voluntarily submitted by the commenter (Eubalaena japonica), ranging in the Commerce.
    [Show full text]